收稿日期: 1997-07-10
修回日期: 1998-01-01
网络出版日期: 1998-08-01
基金资助
"九五"国家攀登计划"青藏高原冰心记录与过去2000年气候变化研究"(项目编号:KZ951-A1-204-02-03)与国家自然科学基金项目"青藏高原冰心中甲烷气体与全球变化研究"(项目编号: 49671021) 资助。
TRACE CARBONACEOUS IMPURITIES FOR CLIMATIC AND ENVIRONMENTAL IMPLICATIONS IN ICE AND SNOW LAYERS
Received date: 1997-07-10
Revised date: 1998-01-01
Online published: 1998-08-01
谢树成,姚檀栋 . 冰雪层中记录气候与环境变化的痕量含碳杂质[J]. 地球科学进展, 1998 , 13(4) : 376 -382 . DOI: 10.11867/j.issn.1001-8166.1998.04.0376
Ice and snow layers are the main information recorders for global changes. The widespread carbonaceous im purities exist in three states of gas, liquid and solid in the layers. The paper summarizes the development of the studies on these carbonaceous impurities for climatic and environmental im plications. The following impurities are discussed as greenhouse gases, high soluble organic acids with low molecular weight, organic pollutants from activities of mankind, spores and pollens, and organic matter with high carbon numbers. Some important study trends on the impurities are presented.
[1] Barnola J M, Raynaud D, Korotkevich T S, et al. Vostok icecore provide 160 000 year record of atmospheric CO2. Nature, 1987, 329:408-414.
[2] Labegrie L D. Changes in the oceanic 13C/12C ratio during the last 140 000 years: high-latitude surface water records.Palaeogeo Palaeoclim Palaeoeco, 1985, 50: 217-240.
[3] Raynaud D, Jouzel J, Barnola J M, et al. The ice record of greenhouse gases. Science, 1993, 259: 926-934.
[4] 姚檀栋. 二氧化碳对气候的影响及气候趋势问题. 地理科学, 1987, 7(2):163-170.
[5] Nisbet F G. The end of ice age. Can J Earth Sci, 1990, 27: 148-157.
[6] Judge A S, Majorowicz J A. Geothermal conditions for gas hydrate stability in the Beaufort-Mackenzie aera: the global change aspect. Palaeogeo Palaeoclim Palaeoeco, 1992, 98: 251-263.
[7] Kvenvolden K A. Gas hydrates Geological perspective and global change. Reviews of Geophysics, 1993, 31(2): 173-187.
[8] Keene W C, Galloway J N. Considerations regarding sources for formic and acetic acids in the troposphere. J Geophys Res,1986, 91: 14 466-14 474.
[9] Maupetit F. Carboxylic acids in high-elevation Alpine glacier snow. J of Geoph Res, 1994, 91(186): 144-166.
[10] Neftel A, Moore E, Oeschger H, et al. Evidence from polar ice cores for the increase in at mospheric CO2 in the past two centuries. Nature, 1985, 315: 45-47.
[11] 秦大河. 南极冰盖表层雪内的物理过程和现代气候及环境记录. 北京:科学出版社, 1995,125-140.
[12] Legrand M, Saigne F C. Methanesulfonic acid in South Polar snow layers: A record of strong El Nino. Geophysical Research Letters, 1991, 18(2): 187-190.
[13] Ivey J P, Davies D M, Morgan V, et al. Methanesulphonate in Antarctic ice. Tellus, 1986, 38B:375-379.
[14] Legrand M, Saigne F C, Saltzman E S, et al. Ice-core record of oceanic emissions of dimethylsulphide during the last climate cycle. Nature, 1991, 350: 144-146.
[15] Anderson C P, Ewing T. Exploring the still unexplored. Nature, 1991, 350:287-288.
[16] Penner J E, Dickinson R E, O'Neil C A. Effects of aerosol from biomass burning on the global radiation budget. Science,1992, 256:1 432-1 433.
[17] Chylek P, Johnson B, Wu H. Black carbon concentration in a Greenland Dye-3 ice core. Geophys Res Lett, 1992, 19: 1 951-1 953.
[18] Lunde G. Organic micropollutants in precipitation in Norway. Atmo Environ, 1977, 11:1 007-1 014.
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